Hydrological research on snowmelt processes in both warm- and cold-climate regions
Hydrological research on snowmelt processes in both warm- and cold-climate regions
批准号:
02454069
负责人:
FUKUSHIMA Yoshihiro
金额:
$4.35万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for General Scientific Research (B)
财政年份:
1990
资助国家:
日本
项目状态:
已结题
起止时间:
1990 至 1992
中文摘要
为了通过热平衡分量阐明融雪过程,评估不同类型森林覆盖对融雪的影响,并估计融雪径流,在不同气候条件下的小流域和样地进行了野外观测,其中包括位于日本中部的京都大学Ashiu实验森林。日本北部的岩手县和日本最北部的北海道大学的莫希里实验森林。用两种超音速风速仪测量了感热通量的体积系数。计算潜热通量和感热通量的热量平衡法与地面积雪融化、蒸发或凝结的观测结果吻合较好,时间间隔1小时,不同区域。将太阳辐射、反照率、长波辐射、地表温度、风速、空气温度和林内相对湿度等热量平衡分量与各开阔地的热量平衡分量进行比较,并确定其差值为开阔地的比值。因此,根据气象观测资料,可以估算出不同海拔、不同坡向、不同坡度、不同森林覆盖度的不同山坡的融雪量。最后,通过这项研究工作变得非常清楚,在不同森林覆盖率和与气候条件无关的地区,融雪季节的径流过程线可以每隔一小时估算一次。
英文摘要
To clarify snowmelt processes by heat balance components, to evaluate effects of various types of forest coverage on snowmelt and to estimate streamflow due to snowmelt, field observations were carried out at a small watershed and at plots in the regions with different types of climate condition, where were Ashiu Experimental Forest of Kyoto University in central Japan, Mt. Iwate in northern Japan and Moshiri Experimental Forest of Hokkaido University in the most north of Japan. Bulk coefficient of sensible heat flux were measured by two types of supper sonic wind-speed meter. Consequently, heat balance method included bulk transfer equation for the estimation of latent heat flux and sensible heat flux shows a good agreement with the observed surface snowmelt, and evaporation or condensation from snow surface, at a time interval of an hour and in various regions. All of heat balance components such as solar radiation, albedo, long-wave radiation, surface temperature, wind-speed, air temperature and relative humidity inside forest were compared with these at each open plot, and its differences were determined as the rations for the values at open plot. Therefore, snowmelt at each hill slope with different altitude, different aspect, different slope angle and different type of forest coverage can be estimated from the meteorological data observed at a point. Finally, it became very clear by this research work that the hydrographs for streamflow in snowmelt season can be estimated in the areas with different forest coverages and no relation to climate condition, at a time interval of an hour.
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白沢 あずみ,福嶌 義宏,鈴木 雅一: "暖候性山地流域における融雪流出の特性" 水文・水資源学会誌.
Azumi Shirasawa、Yoshihiro Fukushima、Masakazu Suzuki:“温暖山区盆地融雪径流的特征”日本水文水资源学会杂志。
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福嶌 義宏(分担執筆): "森林水文学" 文永堂出版, 319 (1992)
福岛义宏(撰稿人):《森林水文学》文内道出版社,319(1992)
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Fukushima,Y.: "Estimation of slreamflow change by global warming in a glacier-covered high mountain avea of the Nepal Himalaya" Pub.of IAHS. 205. 181-188 (1991)
Fukushima,Y.:“全球变暖对尼泊尔喜马拉雅山冰川覆盖的高山大道中流变的估计” Pub.of IAHS。
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Nakashima, T.: "Characteristics of streamflow at a small watershed in steep slope area of Kyoto University forest in Ashiu" Bull. the Kyoto Univ. Forests. 64. 75-87 (1992)
Nakashima, T.:“芦保京都大学森林陡坡区小流域的水流特征”公牛。
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橋本 哲,太田 岳史,福嶌 義宏,大手 信人: "樹種の違いによる林内融雪量の変化について" 日本雪氷学会全国大会講演予稿集. 156-156 (1991)
Satoshi Hashimoto、Takeshi Ota、Yoshihiro Fukushima、Nobuto Ote:“由于树种差异导致森林融雪量的变化”日本冰雪学会全国会议记录 156-156(1991)。
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负责人:FUKUSHIMA Yoshihiro
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